Collaborative Research: Subduction Zone Segmentation over Multiple Seismic Cycles, South-Central Chile

合作研究：智利中南部多个地震周期的俯冲带分割

• 批准号: 1144537
• 负责人: Benjamin Horton
• 金额: $ 17.27万
• 依托单位: University of Pennsylvania
• 依托单位国家: 美国
• 项目类别: Standard Grant
• 财政年份: 2012
• 资助国家: 美国
• 起止时间: 2012-03-15 至 2013-09-30
• 项目状态: 已结题
• 来源: https://www.nsf.gov/awardsearch/showAward?AWD_ID=1144537&HistoricalAwards=false
• 关键词: Collaborative; Research; Subduction; Zone; Segmentation

The possible segmentation of subduction zone faults currently presents one of the most significant questions to the physics and geology of earthquake occurrence and the assessment of future earthquake hazards. How will future large earthquakes be arrayed along a fault? How and why will individual earthquake ruptures stop? Subduction zone faults form the tectonic plate boundaries that parallel the coastlines of many countries around the world. Advances in instrumentation and modeling in recent decades have produced important insights into fault behavior, yet these measurements span only fractions of the time interval between major earthquakes. The goal of this research project is to use an interdisciplinary array of evidence preserved in coastal landforms and sediments to investigate whether segmentation of subduction zone faults is maintained over multiple earthquake cycles spanning hundreds to thousands of years. The field are, the Arauco Peninsula coast of south-central Chile, crosses the boundary between the rupture zones of two of the largest subduction zone earthquakes in the worldwide historic record, on May 22, 1960 (Mw 9.5) and February 27, 2010 (Mw 8.8). Prior to 2010, the study area for this project in south-central Chile was one of the most accepted hard fault segment boundaries along the Peru-Chile trench; it was believed to bound several historical ruptures, including the Great Chilean earthquake of 1960. The Chilean earthquake in February 2010 called this hypothesis into question, when the rupture extended south of this boundary and only partially overlapped with the previous earthquake in AD 1835. The combination of geological evidence of past earthquakes over the last 4000 years, frequent large subduction zone earthquakes, and an unusually long and comprehensive historic record of earthquakes in south-central Chile makes this region a natural laboratory to address fundamental questions about fault segmentation. This research project will test multiple hypotheses regarding earthquake behavior and coastal response: (1) fault ruptures over multiple earthquake cycles could terminate at fixed (hard), variable (soft), or random boundaries, or could include multiple segments; (2) large subduction zone earthquakes will produce a tsunami deposit simultaneous with an abrupt change in land level; and (3) the Holocene coastal evolution in this region reflects a modest net change in relative sea level in which the vertical uplift or subsidence during large earthquakes is largely reversed during the periods between earthquakes. To address these hypotheses the research team will reconstruct vertical land-level changes and tsunami history associated with multiple earthquake cycles using geomorphic, sedimentological and microfossil analysis. They will characterize the optimal environmental settings for the preservation of land-level changes and tsunami deposits in sedimentary sequences and analyze the impacts of these land-level changes on the coastal landscape.Ruptures on subduction zone faults have created some of the largest earthquakes and tsunamis in the world, such as the catastrophic earthquake in Japan in 2011 that killed thousands of people and destroyed coastal cities. The practical importance of this investigation for assessing future earthquake hazards in other similar geological settings was underscored by the unforeseen extent of fault ruptures and resulting earthquake magnitudes in the recent devastating earthquakes in Sumatra in 2004, Chile in 2010 and Japan in 2011. The project will build on strong existing collaboration with Chilean scientists. The results will inform the construction of earthquake and tsunami risk maps through established contacts in Chile, and we will arrange public presentations on earthquake and tsunami hazards. The general concepts will advance knowledge of earthquake behavior over time periods that exceed the relatively short period of the instrumental record.This project is supported by the Tectonics Program and Geomorphology and Land Use Dynamics Program in the Division of Earth Sciences and the Office of International Science and Engineering.

俯冲带断层的可能分段目前是地震发生的物理和地质学以及未来地震危险性评估的最重要问题之一。未来的大地震将如何沿断层排列？个别地震的破裂将如何以及为什么会停止？俯冲带断层形成了与世界上许多国家的海岸线平行的构造板块边界。近几十年来，仪器和建模方面的进步对断层行为产生了重要的见解，但这些测量只跨越了两次大地震之间的一小部分时间间隔。这一研究项目的目标是利用保存在沿海地貌和沉积物中的一系列跨学科证据来调查俯冲带断层的分段是否在跨越数百至数千年的多个地震周期中保持不变。该油田位于智利中南部的阿劳科半岛海岸，跨越了世界历史上有记录以来最大的两次俯冲带地震的破裂带之间的边界，这两次地震分别发生在1960年5月22日(Mw 9.5)和2010年2月27日(Mw 8.8)。在2010年前，该项目位于智利中南部的研究区域是秘鲁-智利海沟沿线最为人所接受的硬断层段边界之一；据信该区域曾发生过几次历史性的断裂，包括1960年的智利大地震。2010年2月的智利地震对这一假设提出了质疑，当时破裂延伸到这条边界以南，只与公元1835年的上一次地震部分重叠。过去4000年来过去地震的地质证据、频繁的大型俯冲带地震以及智利中南部异常漫长和全面的地震历史记录相结合，使该地区成为解决断层分段基本问题的天然实验室。这项研究项目将检验有关地震行为和沿海响应的多个假设：(1)多个地震周期的断层破裂可以终止于固定(硬)、可变(软)或随机边界，或可能包括多个段；(2)大俯冲带地震将在地面水平突变的同时产生海啸沉积；(3)该地区全新世海岸演化反映了相对海平面的适度净变化，其中大地震期间的垂直隆起或沉降在两次地震之间基本逆转。为了解决这些假设，研究小组将利用地貌、沉积学和微化石分析，重建与多个地震周期相关的垂直陆地水平变化和海啸历史。他们将描述在沉积序列中保存陆地平面变化和海啸沉积的最佳环境环境，并分析这些陆地平面变化对沿海景观的影响。俯冲带断层上的构造已经造成了一些世界上最大的地震和海啸，例如2011年发生在日本的灾难性地震，造成数千人死亡，摧毁了沿海城市。在2004年苏门答腊岛、2010年智利和2011年日本发生的破坏性地震中，断层破裂的意外程度和由此产生的震级突显了这项调查对于评估其他类似地质环境下未来地震灾害的实际重要性。该项目将建立在与智利科学家现有的密切合作基础上。结果将通过在智利建立的联系人为地震和海啸风险地图的构建提供信息，我们将安排关于地震和海啸危险的公开陈述。一般概念将在超过仪器记录相对较短的时间段的时间段内促进对地震行为的了解。该项目得到地球科学部和国际科学与工程办公室的构造计划和地貌与土地利用动力学计划的支持。